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Rc3 ocean currents

Date post: 24-May-2015
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Ocean Currents
Transcript
Page 2: Rc3 ocean currents

Warm currents flow away from the equator.

Cold currents flow toward the equator.

Ocean Currents

Page 3: Rc3 ocean currents

SunWindCoriolisGravity

Factors Influencing Currents

Page 4: Rc3 ocean currents

Energy from the Sun heats the water. Warm water is less dense that cold water.

Warm water rises, and cold water sinks.

As warm water rises, cold water moves it to replace it.

Sun

Page 6: Rc3 ocean currents

Just as wind moves from high pressure to low pressure areas, so does the water.

Winds blow across the surface of the water, causing friction.

The water piles up because the surface currents flow slower than the winds.

Wind

Page 8: Rc3 ocean currents

As water piles up and flows from high pressure to low pressure, gravity will pull down on the water.

This forms vertical columns or mounds of water.

The Coriolis Effect causes the water to curve.

Gravity

Page 9: Rc3 ocean currents

Causes water to move to the right in the Northern Hemisphere

Causes water to move to the left in the Southern Hemisphere

The Coriolis Effect

Page 11: Rc3 ocean currents

Make up 10% of oceans’ water Up to maximum depth of 400 m Surface ocean currents are caused by the surface wind patterns.

Surface Currents

Page 13: Rc3 ocean currents

Vertical columns or mounds of water at the surface and flow around them

Produce enormous circular currents Five major locations:

North Pacific - clockwise South Pacific - counterclockwise Indian Ocean - counterclockwise South Atlantic - counterclockwise North Atlantic - clockwise

Gyres

Page 15: Rc3 ocean currents

A strong surface current Begins at the tip of Florida Flows up the eastern coastline of the

U.S. Crosses the Atlantic Ocean Causes warmer climate in NW Europe

Gulf Stream

Page 16: Rc3 ocean currents

Surface waters blow to the right of the wind.

As less dense, surface water moves off shore, cold, deep, denser waters come to the surface to replace them.

Upwelling

Page 18: Rc3 ocean currents

The Great Ocean Conveyor:Helps maintain Earth’s Balance

Page 19: Rc3 ocean currents

Make up about 90% of oceans’ water Differences in density cause them to move. Differences in density are related to

temperature and salinity. At high latitudes, they sink deep into the

ocean basins. Temperatures are so cold, they cause the

density to increase.

Deep Water Currents

Page 20: Rc3 ocean currents

How are ocean currents produced?

Reflective Question

Page 21: Rc3 ocean currents

Abnormally high surface ocean temperatures off the coast of South America

Causes unusual weather patterns across

the globe

El Nino

Page 22: Rc3 ocean currents

Starts because the easterly trade winds weaken and allow the warm waters in the Western Pacific to move east toward South America

This changes where the convection current occurs.

Causing rain where it usually doesn't occur and drought where it usually rains

El Nino

Page 25: Rc3 ocean currents

Abnormally low surface ocean temperatures off the coast of South America

Causes unusual weather patterns across

the globe

La Nina

Page 26: Rc3 ocean currents

Ocean currents move more slowly than winds. Oceans hold more heat than the atmosphere and

land. Cold currents will cause nearby coastlines to be

cooler. Warm currents will cause nearby coastlines to be

warmer.

Where do the cold currents come from? The warm currents?

Ocean’s Effect on Climate

Page 27: Rc3 ocean currents

Predictable Patterns How do these currents affect the climate

of the coastline?

Page 28: Rc3 ocean currents

How do our oceans impact climate?

Reflection Questions


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